In May 1937, shortly after the Hoover Dam was completed and 27 months after Lake Mead started filling, the water level was 1078.70 feet (328.79 meters) above sea level. For 77 years since then, the water level behind the dam has not dropped below 1080 feet. But it just might do that soon.
As the largest reservoir in the United States, Lake Mead is fed mostly by the Colorado River and its tributaries. They are in turn fed by snowmelt from the Rocky Mountains. Lake Mead and the river supply water to farms, businesses, and residents in Nevada, southern California, Arizona, and northern Mexico, and inputs and outflows from the lake are tightly managed by agreements between the surrounding states and Mexico.
According to the U.S. National Park Service and the Bureau of Reclamation, the amount of water flowing out of and evaporating from Lake Mead in recent years has consistently exceeded the amount of water flowing in. To date, Lake Mead has been able to meet the growing demands downstream. The U.S. delivers “about 9 million acre-feet of water to homes, businesses, farms, Native American tribes and communities.” But the trends on Lake Mead something has to change soon in precipitation patterns or water use.
The images at the top of this page were acquired on July 21, 2014, and June 16, 2013, by the Operational Land Imager on the Landsat 8 satellite. Both images show the lake at its south end, near Hoover Dam. Differences in water color could be a difference in the amount of suspended sediment or a result of slightly different lighting. Shorelines retreated over the year, and islands in the middle of the lake continue to grow as water recedes. Turn on the image comparison tool to spot the differences. View our 2003 feature story to see how much has changed since 2000.
The graph above shows the steadily declining water level at Hoover Dam. In January 2013, water levels were 1122.32 feet. As of July 30, 2014, the water stood at 1080.69 feet. Regional water management plans call for water restrictions to kick in when lake levels drop below 1075 feet (328 meters).
The southwestern United States and the Colorado River basin have been coping with varying levels of drought for most of the past fourteen years. The river collects most of its water from melting snow each spring and summer, but the winter supplies have been uneven and generally below average. As a result, the water stored in the two great reservoirs of the region—Lake Powell and Lake Mead—has been declining slowly but steadily.
At full capacity, the level of Lake Mead is 1229.00 feet (374.60 meters), a number it has not approached since the early 1980s. On the downside, water has dropped below 1,100 feet on just three occasions since Hoover Dam was created: during a serious drought from 1955–1957; when Lake Powell was created (and upstream water flow slowed) in 1964–1965; and late in 2010, during the current drought.
- Bureau of Reclamation, Lower Colorado Region (2014, July 31) Accumulations for July 2014. Accessed July 31, 2014.
- Bureau of Reclamation, Lower Colorado Region (2014, July 8) Lake Mead Levels Drop to Historic Lows. Accessed July 31, 2014.
- Bureau of Reclamation, Lower Colorado Region (2014, July 1) Lake Mead at Hoover Dam, Elevation (monthly). Accessed July 31, 2014.
- NASA Earth Observatory (2010, September 23) Water Level Changes in Lake Mead.
- NASA Earth Observatory (2003, November 13) Drought Lowers Lake Mead.
- National Park Service Low Water—Lake Mead National Recreation Area. Accessed July 31, 2014.
NASA Earth Observatory image by Robert Simmon, using Landsat data from the U.S. Geological Survey. Caption by Michael Carlowicz.
- Landsat 8 - OLI